IIIFカラー高解像度
国立情報学研究所 - ディジタル・シルクロード・プロジェクト
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| IIIFカラー高解像度 |
| Scientific Results of a Journey in Central Asia, 1899-1902 : vol.4 | |
| 1899-1902年の中央アジア旅行における科学的成果 : vol.4 |
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引用情報
WESTWARDS TO LADAK.
238
Fig. 131. LOOKING NORTH FROM CAMP CXXVIII.
there was another latitudinal valley, running in the same direction. Possibly it would be more correct to regard these side-glens as transverse glens; in any case they appear to open out upon the big depression of the southern latitudinal valley.
At this camp there was scarce a trace of grazing, beyond an occasional scrubby plant on this or the other slope. The rock in this region was the same as hitherto, limestone; at the beginning of the day's march it dipped 47° towards the S. 31° E.
In this part of Tibet it is an unusual sound to hear the ripple of water, so that even the small quantity which the Raga-tsangpo was then carrying produced the impression of an actual river, although in the peripheral moun
tain regions it would simply be called a very insignificant brook. But in this respect this region itself will present quite a different appearance in the summer, for then the entire surface may be as wet as a sponge and large areas of the latitudinal valleys will be more like marshes. It was however a disagreeable region, and bitterly cold, because of a raw icy current of air which flowed uninterruptedly down the valley.
Fig. 132. LOOKING W FROM CAMP CXXVIII.
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